The research team, led by Qiumei Teng and Tao Ding of the Guangxi Institute of Botany, systematically examined tree height, diameter at breast height (DBH), soil physicochemical properties, enzyme activity, and microbial communities at four elevations: 1,750, 1,850, 1,950, and 2,050 meters. Contrary to the simple expectation that warmer, lower elevations would always produce the tallest trees, the fir exhibited a pronounced non-linear trajectory. Tree height and DBH were highest at 1,750 meters, lowest at 1,850 meters, and then partially recovered toward 2,050 meters. The DBH at 1,750 meters was 72.0 percent higher than at 1,850 meters, while tree height was 54.5 percent higher at the lowest elevation. Similar non-monotonic growth patterns with altitude have been observed in Norway spruce and Canary pine, supporting the view that tree growth responses to elevation are context-dependent rather than simply increasing or decreasing with height.

What explains the mid-elevation growth dip? The answer appears to lie in the soil. At 1,850 meters, soil water content was the highest of all sampled elevations, while total phosphorus (TP) and total potassium (TK) contents were the lowest. The researchers speculate that this mid-elevation moisture peak may coincide with a regional cloud belt or fog zone, where persistent low clouds and frequent fog deposition supply substantial non-rainfall water directly to the soil surface. High soil moisture can lead to poor aeration, facilitate pathogen breeding, and cause excessive leaching of nutrients such as phosphorus and potassium. The negative correlation between soil water content and TP observed in the study supports this mechanism. Moreover, the carbon-to-phosphorus and nitrogen-to-phosphorus ratios at 1,850 meters exceeded global forest averages, suggesting potential phosphorus limitation based on stoichiometric inference.

Phosphorus is a critical nutrient for root development, photosynthesis, and biomass accumulation. Adequate phosphorus supports greater tree height and leaf area, whereas phosphorus deficiency restricts growth by impairing rRNA synthesis, protein translation, and cell division. The structural equation modeling (SEM) revealed that TP had a significant positive direct effect on plant growth (β = 0.61, p < 0.05) and on bacterial diversity (β = 0.36, p < 0.05), but significant negative direct effects on microbial composition (β = −0.49), fungal life-history strategy (β = −0.41), and microbial network complexity (β = −0.37). These opposing pathways illustrate how a single factor can simultaneously benefit plants and bacteria while reshaping fungal communities through altered competitive hierarchies among fungal functional groups.

The study also revealed striking elevational patterns in microbial diversity and community assembly. The Chao1, ACE, and Shannon indices for both soil bacterial and fungal communities were lowest at 1,850 meters, closely linked to the low TP content at this elevation, as low phosphorus availability is known to restrict microbial growth and diversity in forest soils. Fungal community assembly was predominantly deterministic at 1,750 meters—the elevation where plant growth peaked—suggesting intensified environmental filtering under warm, humid conditions with higher resource availability. In contrast, bacterial communities remained stochastically assembled across all elevations, likely due to higher bacterial dispersal rates, smaller body sizes, greater metabolic flexibility, and lower competitive exclusion. The researchers caution that these assembly conclusions are based exclusively on the phylogenetic normalized stochasticity ratio (NST), which does not account for phylogenetic or functional relationships, so deterministic signals driven by trait-based selection may be overlooked.

Perhaps the most compelling finding concerns microbial life-history strategies. According to the oligotrophic-copiotrophic framework, copiotrophs (r-strategists) thrive in nutrient-rich, high-carbon environments, whereas oligotrophs (K-strategists) dominate under low-nutrient conditions. For fungi, Basidiomycota was taken as representative of an oligotrophic lifestyle and Ascomycota as copiotrophic. At 1,850 meters, the fungal oligotroph-to-copiotroph ratio was the highest, consistent with the peak abundance of Basidiomycota under phosphorus- and potassium-limited conditions. Conversely, the bacterial oligotroph-to-copiotroph ratio was lowest at this elevation, reflecting copiotroph enrichment likely due to bacterial adaptation to phosphorus limitation via phosphatase secretion. Critically, the SEM showed that fungal life-history strategy had the strongest negative direct effect on plant growth (β = −0.52, p < 0.05), indicating that the dominance of oligotrophic fungi in a phosphorus-poor environment was unfavorable for the fir.

The study also examined cross-kingdom co-occurrence networks built with the MENA pipeline using Random Matrix Theory. The complexity of bacterial-fungal networks increased with elevation: networks at higher elevations were smaller in scale, with fewer nodes and edges, but characterized by a significantly higher proportion of negative links. This pattern suggests that while high-elevation environments constrain network size, they also intensify competitive interactions within the network. The proportion of negative connections is often interpreted as a proxy for competitive exclusion or niche partitioning. Under increasing environmental stress, a higher proportion of negative connections may indicate intensified competition, but it can also arise from non-competitive processes such as environmental filtering. Tree height decreased with increasing network complexity, and the researchers propose that greater complexity may reduce nutrient mineralization and plant-growth-promoting functions due to intensified competition for resources and energy among microbial taxa, ultimately forming a competitive network that suppresses plant growth.

The researchers emphasize that these findings underscore how soil physicochemical properties and microbial communities jointly determine the growth of endangered mountain plants along altitudinal gradients. Although bacterial and fungal diversity exert distinct effects on plant growth—tree height and DBH increased with bacterial diversity but showed no significant correlation with fungal diversity—their life-history strategies should be considered a critical factor in managing endangered species. The lack of a significant fungal diversity effect may reflect opposing influences of beneficial mycorrhizal and pathogenic fungi counterbalancing each other, or growth being governed by specific functional groups rather than overall diversity. Tree height and DBH increased with the relative abundance of Ascomycota but declined as Basidiomycota rose, partially supporting the hypothesis that interactions between soil properties and microbial life-history strategies influence fir growth.

The study acknowledges several limitations. The co-occurrence results should be viewed as preliminary descriptive patterns rather than robust quantitative descriptions of community structure, as the networks are based on statistical analysis and do not directly demonstrate real biological interactions. The SEM was constructed with a limited effective sample size (n = 12), which may limit statistical power and generalizability. Temperature, another critical driver of soil microbial activity and plant growth, was not directly measured during sampling. Samples were collected only in December 2022, providing a winter snapshot that cannot capture seasonal dynamics. Phosphorus limitation was inferred indirectly from TP and stoichiometric ratios, requiring direct empirical validation. Future studies incorporating manipulative experiments such as transplantation and warming are critically needed to test these factors and partition the relative contributions of abiotic versus biotic drivers along elevational gradients.

Despite these caveats, the research provides a new perspective for the ex situ conservation and in situ management of endangered plants. The study suggests that 1,750 meters is the optimal elevation for Abies yuanbaoshanensis growth, whereas growth at 1,850 meters tends to be lower, partly explained by elevated soil water content and reduced availability of total phosphorus and potassium. The causal chain highlights that water-mediated phosphorus limitation not only directly impairs plant nutrition but also indirectly affects growth by restructuring soil fungal communities toward oligotrophic dominance and intensifying competitive interactions within the microbial network. These findings suggest that altitudinal zones and associated soil conditions must be prioritized in conservation efforts—suitable habitats are critical for expanding wild populations, while assessments of soil nutrients and microbial communities are essential for ex situ conservation. As climate change continues to intensify anomalies in high-elevation habitats, understanding the belowground microbial life that sustains this ancient relict fir may prove decisive for its survival.

Subject of Research: Soil microbial life-history strategies influence endangered fir growth across elevations

Article Title: Endangered plant growth was influenced by soil microbial life-history strategies across elevations

Article References: Teng, Q., Wang, Y., Lyu, S., Wei, J., Xu, G., & Ding, T. (2026). Endangered plant growth was influenced by soil microbial life-history strategies across elevations. Frontiers in Microbiology, 17, Article 1922651. https://doi.org/10.3389/fmicb.2026.1922651

Image Credits: AI Generated

DOI: 10.3389/fmicb.2026.1922651

Keywords: Abies yuanbaoshanensis, elevation, endangered plant, microbial life strategy, soil microbial community, phosphorus limitation, co-occurrence networks, conservation, Endangered, plant, growth, influenced